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  • Seawater  (2)
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  • 1
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2000-05-08
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Paytan, A -- New York, N.Y. -- Science. 2000 Apr 28;288(5466):626-7.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geological and Environmental Sciences, Stanford University, Braun Hall, Building 320, Stanford, CA 94305, USA. apaytan@pangea.stanford.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/10798999" target="_blank"〉PubMed〈/a〉
    Keywords: *Atmosphere ; *Evolution, Chemical ; Geologic Sediments/*chemistry ; Iron/chemistry ; Oxidation-Reduction ; *Oxygen ; Seawater ; Sulfates/*chemistry/metabolism ; Sulfides/chemistry/metabolism ; Sulfur Isotopes ; Sulfur-Reducing Bacteria/metabolism ; Temperature
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2017. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 18 (2017): 3946–3963, doi:10.1002/2017GC007071.
    Description: The sources of terrestrial material delivered to the California margin over the past 7 Myr were assessed using 187Os/188Os, Nd, and Pb isotopes in hydrogenetic ferromanganese crusts from three seamounts along the central and southern California margin. From 6.8 to 4.5 (±0.5) Ma, all three isotope systems show more radiogenic values at Davidson Seamount, located near the base of the Monterey Canyon System, than in Fe-Mn crusts from the more remote Taney and Hoss Seamounts. At the Taney Seamounts, approximately 225 km farther offshore from Davidson Seamount, 187Os/188Os values, but not Pb and Nd isotope ratios, also deviate from the Cenozoic seawater curve toward more radiogenic values from 6.8 to 4.5 (±0.5) Ma. However, none of the isotope systems in Fe-Mn crusts deviate from seawater at Hoss Seamount located approximately 450 km to the south. The regional gradients in isotope ratios indicate that substantial input of dissolved and particulate terrestrial material into the Monterey Canyon System is responsible for the local deviations in the seawater Nd, Pb, and Os isotope compositions from 6.8 to 4.5 (±0.5) Ma. The isotope ratios recorded in Fe-Mn crusts are consistent with a southern Sierra Nevada or western Basin and Range provenance of the terrestrial material which was delivered by rivers to the canyon. The exhumation of the modern Monterey Canyon must have begun between 10 and 6.8 ± 0.5 Ma, as indicated by our data, the age of incised strata, and paleo-location of the Monterey Canyon relative to the paleo-coastline.
    Description: Funding was provided by the United States Geological Survey Pacific Coastal and Marine Science Center Marine Minerals Group, the University of California Santa Cruz Scholarship for Re-Entry Women in Science, and the UCSC Earth and Planetary Science Department Waters Award.
    Description: 2018-05-15
    Keywords: Ferromanganese crusts ; Osmium isotopes ; Neodymium isotopes ; Lead isotopes ; Monterey Canyon System ; Seawater
    Repository Name: Woods Hole Open Access Server
    Type: Article
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